$\"fracture\"$ <\/a>A fracture<\/strong> is the separation of an object or material into two or more pieces under the action of stress. Engineers need to understand fracture mechanisms. Some fractures<\/strong> (e.g., brittle fractures<\/strong>) occur under specific conditions without warning<\/strong> and can cause major damage<\/strong> to materials. A brittle\u00a0fracture<\/strong> occurs suddenly and catastrophically without any warning, resulting in spontaneous and rapid crack propagation<\/strong>. However, for ductile fracture, the presence of plastic deformation warns that failure is imminent, allowing preventive measures to be taken. Studying fracture mechanics<\/strong> may assist in understanding how fracture occurs in materials.<\/p>\n

In the tensile test, the fracture point<\/a> is the point of strain where the material physically separates. At this point, the strain reaches its maximum value, and the material fractures, even though the corresponding stress may be less than the ultimate strength. Ductile materials<\/strong> have a fracture strength lower than the ultimate tensile strength<\/a> (UTS), whereas, in brittle materials, the fracture strength is equivalent to the UTS. If a ductile material reaches its ultimate tensile strength in a load-controlled situation, it will continue to deform, with no additional load application, until it ruptures. However, if the loading is displacement-controlled, the deformation of the material may relieve the load, preventing rupture. It is possible to distinguish some common characteristics among the stress-strain curves of various groups of materials. On this basis, it is possible to divide materials into two broad categories; namely:<\/p>\n

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Ductile Materials<\/strong>. Ductility is the ability of a material to be elongated in tension. Ductile material will deform (elongate) more than brittle material. Ductile materials show large deformation before fracture. In ductile fracture<\/strong>, extensive plastic deformation (necking) takes place before fracture. Ductile fracture<\/strong> (shear fracture) is better than brittle fracture because there is slow propagation and an absorption of a large amount of energy before fracture. Any fracture process involves two steps, crack formation and propagation, in response to an imposed stress. The mode of fracture is highly dependent on the mechanism of crack propagation. Cracks in ductile materials are said to be stable (i.e., resist extension without an increase in applied stress). For brittle materials, cracks are unstable. That means crack propagation, once started, continues spontaneously without an increase in stress level. Ductility is desirable in the high temperature and high-pressure applications in reactor plants because of the added stresses on the metals. High ductility in these applications helps prevent brittle fracture.<\/li>\n
Brittle Materials<\/strong>. When stress subjects, brittle materials break with little elastic deformation and without significant plastic deformation. Brittle materials absorb relatively little energy before fracture, even high-strength materials. In brittle fracture<\/strong> (transgranular cleavage<\/strong>), no apparent plastic deformation takes place before fracture. In crystallography, cleavage is the tendency of crystalline materials to split along definite crystallographic structural planes. Any fracture process involves two steps, crack formation<\/strong> and propagation<\/strong>, in response to an imposed stress. The mode of fracture is highly dependent on the mechanism of crack propagation. For brittle materials<\/strong>, cracks are unstable<\/strong>. That means crack propagation, once started, continues spontaneously without an increase in stress level. Cracks propagate rapidly (speed of sound) and occur at high speeds – up to 2133.6 m\/s in steel. It should be noted that smaller grain sizes<\/a>, higher temperatures, and lower stress tend to mitigate crack initiation. Larger grain sizes, lower temperatures, and higher stress favor crack propagation. A stress level below which a crack will not propagate at any temperature. This is called the lower fracture propagation stress. For brittle fracture, the fracture surface is relatively flat and perpendicular to the direction of the applied tensile load. In general, a brittle fracture requires three conditions:\n
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Flaw such as a crack<\/li>\n
Stress is sufficient to develop a small deformation at the crack tip<\/li>\n
The temperature at or below DBTT<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n
See also: Ductile-brittle Transition Temperature<\/a><\/p>\n
See also: Stress-corrosion Cracking<\/a><\/p>\n
See also: Hydrogen Embrittlement<\/a><\/p>\n<\/div><\/div>\n
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<\/span>References:<\/div>
Materials Science:<\/strong>\n\n
U.S. Department of Energy, Material Science. DOE Fundamentals Handbook, Volume 1 and 2. January 1993.<\/li>\n
U.S. Department of Energy, Material Science. DOE Fundamentals Handbook, Volume 2 and 2. January 1993.<\/li>\n
William D. Callister, David G. Rethwisch. Materials Science and Engineering: An Introduction 9th Edition, Wiley; 9 edition (December 4, 2013), ISBN-13: 978-1118324578.<\/li>\n
Eberhart, Mark (2003). Why Things Break: Understanding the World by the Way It Comes Apart. Harmony. ISBN 978-1-4000-4760-4.<\/li>\n
Gaskell, David R. (1995). Introduction to the Thermodynamics of Materials (4th ed.). Taylor and Francis Publishing. ISBN 978-1-56032-992-3.<\/li>\n
Gonz\u00e1lez-Vi\u00f1as, W. & Mancini, H.L. (2004). An Introduction to Materials Science. Princeton University Press. ISBN 978-0-691-07097-1.<\/li>\n
Ashby, Michael; Hugh Shercliff; David Cebon (2007). Materials: engineering, science, processing, and design (1st ed.). Butterworth-Heinemann. ISBN 978-0-7506-8391-3.<\/li>\n
J. R. Lamarsh, A. J. Baratta, Introduction to Nuclear Engineering, 3d ed., Prentice-Hall, 2001, ISBN: 0-201-82498-1.<\/li>\n<\/ol>\n<\/div><\/div><\/div>
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See above:<\/h2>\n
Toughness<\/i> <\/span><\/a><\/p><\/div><\/div>
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